• 제목/요약/키워드: Partially Thick Volume

검색결과 3건 처리시간 0.016초

부분적으로 후육부를 가지는 평판형 제품의 제작을 위한 사출성형 금형의 냉각채널 설계에 관한 연구 (A Study on the Design of Cooling Channels of Injection Mould to Manufacture a Flat Part with a Partly Thick Volume)

  • 안동규;박민우;김형수
    • 한국정밀공학회지
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    • 제29권8호
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    • pp.824-833
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    • 2012
  • The shrinkage and the warpage of the moulded part are influenced by the design of the product and injection mould. In a flat part with a partly thick volume, the warpage of the flat part is created from the difference of the shrinkage between thin and thick regions. The warpage of the flat part with a partly thick volume can be reduced by a proper design of the cooling system in the injection mould. The goal of this paper is to design properly cooling channels of injection mould to manufacture a flat part with a partly thick volume. The conformal cooling channel is adopted to improve cooling characteristics of a region with the thick volume. The linear cooling channels are assigned to the other region. The proper design of the conformal cooling channels is obtained from three-dimensional injection molding analysis for various design alternatives. The moulding characteristics of the designed mould with both conformal and linear cooling channels are compared to those of the mould with linear cooling channels from viewpoints of temperature, shrinkage and warpage of the moulded part using numerical analysis. Injection mould with both conformal and linear cooling channels for the flat part with a partially thick volume is fabricated. In addition, injection moulding experiments are performed using the fabricated mould. From the results of the injection moulding experiments, it has been shown that the designed mould can successfully fabricate the flat part with a partially thick volume.

Paleo-Tsushima Water influx to the East Sea during the lowest sea level of the late Quaternary

  • Lee, Eun-Il
    • 한국지구과학회지
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    • 제26권7호
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    • pp.714-724
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    • 2005
  • The East Sea, a semi-enclosed marginal sea with shallow straits in the northwest Pacific, is marked by the nearly geographic isolation and the low sea surface salinity during the last glacial maximum (LGM). The East Sea might have the only connection to the open ocean through the Korea Strait with a sill depth of 130 m, allowing the paleo-Tsushima Water to enter the sea during the LGM. The low paleosalinity associated with abnormally light $\delta^{18}O$ values of planktonic foraminifera is interpreted to have resulted from river discharge and precipitation. Nevertheless, two LGM features in the East Sea are disputable. This study attempts to estimate volume transport of the paleo-Tsushima Water via the Korea Strait and further examines its effect on the low sea surface salinity (SSS) during the lowest sea level of the LGM. The East Sea was not completely isolated, but partially linked to the northern East China Sea through the Korea Strait during the LGM. The volume transport of the paleo-Tsushima Water during the LGM is calculated approximately$(0.5\~2.1)\times10^{12}m^3/yr$ on the basis of the selected seismic reflection profiles along with bathymetry and current data. The annual influx of the paleo-Tsushima Water is low, compared to the 100 m-thick surface water volume $(about\;79.75\times10^{12}m^3)$ in the East Sea. The paleo-Tsushima Water influx might have changed the surface water properties within a geologically short time, potentially decreasing sea surface salinity. However, the effect of volume transport on the low sea surface salinity essentially depends on freshwater amounts within the paleo-Tsushima Water and excessive evaporation during the glacial lowstands of sea level. Even though the paleo-Tsushima Water is assumed to have been entirely freshwater at that time period, it would annually reduce only about 1‰ of salinity in the surface water of the East Sea. Thus, the paleo-Tsushima Water influx itself might not be large enough to significantly reduce the paleosalinity of about 100 m-thick surface layer during the LGM. This further suggests contribution of additional river discharges from nearby fluvial systems (e.g. the Amur River) to freshen the surface water.

조영 증강 자기공명정맥 촬영술에서의 동맥과 정맥 triggering 방법의 비교 (Contrast Enhanced Cerebral MR Venography: Comparison between Arterial and Venous Triggering Methods)

  • 장민지;최현석;정소령;안국진;김범수
    • Investigative Magnetic Resonance Imaging
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    • 제16권2호
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    • pp.152-158
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    • 2012
  • 목적: 뇌내 정맥혈관을 평가하기 위한 조영 증강 자기공명 정맥촬영술의 arterial trigger 와 venous trigger 방법으로 시행한 영상의 차이점을 비교 분석하고자 한다. 대상과 방법: 건강검진을 목적으로 자기공명정맥촬영술을 시행한 41명의 환자들을 대상으로 해면부위의 내경 동맥에서 arterial triggering하여 6초 후에 얻은 영상 (n = 20) 과 상시상 정맥동에서 venous triggering (n = 21) 방법으로 시행한 영상을 후향적으로 분석하였다. 영상은 가돌리늄 조영제 ($Magnevist^{(R)}$, Schering, Germany)를 0.1 mmol/kg 정맥주입하여 시행하였고, 두개강 전반에 대하여 시상영상을 fast spoiled gradiend echo sequence로 시행하였다 (TR/TE 5.2/1.5, matrix $310{\times}310$, 절편수 124 절편, 두께 15 cm). 두 그룹의 영상을 해부학적 정맥 혈관 구조에 따라 17 정맥구역에 대하여 평가하였고, 정맥의 영상품질은 세 단계 (안보임, 일부 보임, 완전히 보임)로 나눠서 평가하였다. 결과: 정맥이 완전히 보인 구역은 arterial triggering 자기공명 정맥 촬영술에서 84% (272/323), venous triggering 자기 공명 정맥촬영술에서 91% (310/340) 이다. Venous triggering 자기공명촬영술과 arterial 자기 공명 정맥촬영술을 비교하였을 때 뇌내 정맥 구조를 평가하는데 있어 venous triggering 방법이 통계적으로 유의하게 높았다 (Fisher exact test, p<0.006). 결론: 조영 증강 자기공명 정맥 촬영술은 정맥 혈관 구조에 대한 고화질의 이미지를 제공하였고 arterial triggering 방법보다 venous triggering 방법이 뇌내 정맥 구조 평가에 우월한 것으로 나타났다.